Master of Science Focus: Structural Geology and Mapping Kent State University – Kent, Ohio 8/2009 - 5/2015 Bachelor of Science Honors: Cum Laude Major: Geology Minor: Geographic Information
Earthquakes are best described as a shaking or vibration of the ground caused by breaking of rock. Sometimes they are very strong and other times you would hardly notice them. This shaking occurs when stress that builds up in the crust is suddenly released as the crust breaks free and/or slides against the other pieces of crust. Earthquakes may also be thought of as the breaking of a popsicle stick by applying pressure to both ends at the same time. Should you try this experiment , you will feel
phases of the Himalayan orogeny in the late Cenozoic time; the occurrence of the thick, incompetent Salt Range formation at the base of the sedimentary sequence has strongly influenced the structure. 5.2 GENERAL STRUCTURES OF THE PAIL-BAHDRAR AREA Structural features were essentially the result of gravitative flow process (a tectonic diaprisim) involving the subsurface flow of highly incompetent sequence of the Salt Range formation, which consists of red crystalline gypsiferrous marls, gypsum, anhydrite
Writing 1 I begin my hike in comfortable clothes, a camelbak, flashlight and my ticket to view the caves. The first thing I see is the large rockslide above the visitor’s center. The rockslide is called talus slop. A talus slope describes a type of rockslide that is a loose debris piles. Talus slopes have mild to moderate rockslides as rocks slide down the pile. I was surprised when one such rock hit my head dead center. Facing the American Fork Canyon in the Wasatch Mountains of Utah, USA I see
Faults are a break in the crust of a body like the earth or moon along with some movement of rock taking place. The hard outer layer that makes up the earth’s surface is called crust. It floats on a bed of semi-molten rock and is cracked in places. Each one of the cracked sections of the crust is called a plate. Scientists call the places where earth movement has left cracks in the surface rock faults. Evidence of shifting plates and released stress of moving solid rock seen by broken crust on
Area of the Long Point Fault The Long Point Fault is located in Harris County, which covers 83,450 square miles located with in Houston, Teaxas City Limits. Research specifies that there are three sections of the Long Point fault that appear to be active; some sections of the Long Point fault have averaged more than 2 cm per year of vertical offset over the last 20 years. Evidence of the faults concludes it is a natural fault. The reason for activity is not caused by man, even though man’s activities
Espinoza J15040959 05.19.17 GLY1010 Geology Assignment 1. Mineralogy - This field is the science that studies minerals, their crystalline and structures, and their properties. A mineralogist should be working on being able to know the properties of minerals by studying and testing them. INTERNET RESOURCES: https://www.merriam-webster.com/dictionary/mineralogy http://www.environmentalscience.org/career/mineralogist 2. Igneous Petrology - It is the part of geology that is in charge of the study of
When people think of geology, they usually think of rocks and fossils. However, geology is actually a very large field of study. The knowledge of geologists ranges from rocks and fossils to the moon and other planets (Hammonds 7-8). Geologists use a variety of subjects in their work, but the sciences and math are the most important. Some of the sciences geologists study are physics and chemistry (12). English is also a subject that geologists use when communicating with other scientists, the
upwards ... ... middle of paper ... ...eology. 16 (12), p1108-1111. Paterson, S., and Tobisch, O. (1992). Rates of processes in magmatic arcs: implications for the timing and nature of pluton emplacement and wall rock deformation. Journal of Structural Geology. 14 (3), p291-300. Schaltegger, U., Zeilinger, G., Frank, M., and Burg, J-P. (2002). Multiple mantle sources during island arc magmatism: U–Pb and Hf isotopic evidence from the Kohistan arc complex, Pakistan. Terra Nova. 14 (6), p461-468
I am applying to the MSc degree program in Geology at the Department of Earth and Environmental Sciences, Ludwig Maximilian University of Munich, starting in winter 2014. My previous education and work experience as an exploration geologist make me a good candidate for this program. I have a strong research interest in understanding different Earth’s Lithosphere and plate boundary processes in relation to petrogenesis, mechanisms of rock deformation and metamorphism, and dynamics of crustal fluid
The Franciscan Complex Introduction The Franciscan Terrane of central California represents an accretionary complex formed by long-term subduction of an oceanic plate under the Western margin of the North American craton. The Franciscan complex is composed of three distinguishable belts: the eastern belt (Yolla Bolly and Pickett Peak terranes), the central belt, and the coastal belt. Age and metamorphic grade of the belts decreases to the west (Blake and Jones, 1981). Formation of the accretionary
workings of the earth, due to the nature of the seismic waves they produce. P and S waves are reflected and refracted at different boundaries within the earth, and this enables seismologists to make inferences about the internal composition and structural of planet Earth. (Merali and Skinner, 2009, p.252). In 1906, a scientist by the name of Richard Dixon Oldham had suggested a theory structured another scientists findings by the name of Emil Wiechert. Oldham had identified that S waves and P waves
Seismic Resolution The definition of the term thin bed involves the concept of the resolving power (Widess, 1973) thus seismics is impacted by resolution. Most geological structures have a smaller vertical dimension than a horizontal one (Chang et al, 1996), thus, the ratio of the vertical dimensions plays a very important role in seismic resolution. As the dimension ratio decreases, the difficulty in identifying geological events increases and become more challenging (Chang et al, 1916). Sheriff
people. II. Petroleum Petroleum "occurs in a liquid phase as crude oil and condensate and in a gaseous phase as natural gas" (Petroleum Geology, 2003). The development of petroleum in gaseous phase is largely dependent on the "kind of source rock from which the petroleum was formed and the physical and thermal environment in which it exists" (Petroleum Geology, 2003). Petroleum is commonly identified as the crude oil, in liquid form, which is found deep below the ground surface around less than
Rising of the earth’s crust is responsible for producing earthquakes, Submission of report for publishing. Earthquake is caused due to the movement of the land is a myth. The most important thing that is missing in this view is that there is no explanation for why earthquake occurs in the center of the land instead of the peripheral area. Actually the land is rising in different places. This is the reason why earthquakes occur only in the central parts of the land. To be specific, after
subsequently constrained to skim the entire book. From what I did gather this is a very well written book, incredibly detailed, by someone who is clearly well educated in Latin American History as well as military tactics and it seems as though, geology and geography as well. The amount of imagery and detail that was put into the chapter on land alone was enough to fill it’s own book. “…an unlooked-for picture awaits the traveler … all of which confers upon the landscape in a fuse in a distant and
because of the quality of its doubt. Its Faith is a poor thing, but its doubt is a very intense experience. The first aspects of science that seem to interest Tennyson were astronomy. However, he seemed to become more interested in geology and Lyell’s work on Geology. Sir Charles Lyell, is perhaps the most significant figure ever born in Angus, Scotland. On the fourteenth of November 1797 Charles Lyell was born. His father, Charles Lyell, enrolled in 1786 at St. Andrew University where he studied
The Fundamental Principles of Relative DatingRelative dating involves placing events in their proper chronological sequence, that is, in the order of their occurrence (Dutch 1998). This type of dating tells us which geologic event happened first, but does not give an exact date to which something happened. There are several different methods that are used in relative dating. These are the fundamental methods that are used in the field by geologists' and earth scientists to gather information about
conjecture. He contended that the plates at one point formed one large continent called Pangea, which allowed like fossils and rock types to become closer together, which broke apart. Despite how well the continents fit together and the facts about the geology, the general public would not accept Wagener’s proposal. This is largely due to religious conflicts and the lack of evidence presented to them. The earth’s surface and the mantle make up the composition of the tectonic plates. This layer, called
World history is defined as the study of the relationships between people and different aspects of society such as culture, behavior, freedom and religion (Manning,2003,1). Two factors have had a significant impact on world history, are external and internal factors (World History Connected, n.d). The external factors are based on scientific principles in areas such as chemistry, archaeology and the environment , internal factors are traditional topics of history such as slavery, freedom, abolition